The interaction of katabatic winds and mountain waves
Description:
The variation in the oft-observed, thermally-forced, nocturnal katabatic winds along the east side of the Rocky Mountains can be explained by either internal variability or interactions with various other forcings. Though generally katabatic flows have been studied as an entity protected from external forcing by strong thermal stratification, this work investigates how drainage winds along the Colorado Front Range interact with, in particular, topographically forced mountain waves. Previous wor…
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Date:
January 1, 1997
Creator:
Poulos, G.S.
Partner:
UNT Libraries Government Documents Department